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DAILY PRECIPITATION FROM STATISTICAL RECONSTRUCTIONS (Serreze)
SummaryProviding rapid updates of gridded precipitation fields is difficult due to the degradation of the station network. Starting about 1990, many stations in the Former Soviet Union (FSU) and Canada closed. Canada is also seeing a trend toward automation. In recognition, we are providing updated fields using statistical techniques. This reconstruction technique has also been used to compile fields back to 1980 to provide a period of overlap with gridded fields based on interpolation of monthly station precipitation and daily disaggregation (see DAILY PRECIPITATION, FROM MONTHLY STATION RECORDS AND DISAGGREGATION). The reconstructions employ a four-step approach. As part of the data processing of ArcticRIMS (http://RIMS.unh.edu) based at the Water Systems Analysis Group, University of New Hampshire all data sets have been aggregated to multiple temporal and spatial resolutions.
The data is presented in 24 sub-datasets of different spatial and temporal
aggregations (see aggregation description below).
Data AccessORDER data for delivery by FTP.
* - This Dataset was submitted to or acquired by ArcticRIMS from a third party Research Institution. Data AggregationThere are two distinct methods to produce data aggregation along the "time" axis of the cube. These are -
Each aggregated data file in a dataset has a notation of a method (mean or sum) used to produce the file. The notation included in the first (top) line of the file. Please, pay attention to that. Aggregation along the "spatial scale" axis of the cube is
done using simple mean (average) over all grid cells of each basin (river, sea
basin, or continent) from an appropriate grid cell file. Additional Information
Temporal Coverage
Spatial CoverageMinimum latitude: 45.00000000, Minimum longitude: -180.00000000Maximum latitude: 90.00000000, Maximum longitude: 180.00000000
Point of Contact
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